HYDRAULIC CONDUCTIVITY, BULK DENSITY, MOISTURE CONTENT, AND ELECTRICAL CONDUCTIVITY OF A NEW SANDY LOAM FEEDLOT SURFACE

2001 ◽  
Vol 17 (4) ◽  
Author(s):  
M. C. McCullough ◽  
D. B. Parker ◽  
C. A. Robinson ◽  
B. W. Auvermann
Keyword(s):  
Electrical Conductivity ◽  
Hydraulic Conductivity ◽  
Moisture Content ◽  
Bulk Density ◽  
Sandy Loam

Effects of tillage and direct drilling on soil properties during the growing season in a long-term barley mono-culture system

1977 ◽  
Vol 88 (2) ◽  
pp. 431-442 ◽  
Author(s):  
J. D. Pidgeon ◽  
B. D. Soane
Keyword(s):  
Moisture Content ◽  
Bulk Density ◽  
Management Practices ◽  
Sandy Loam ◽  
Spring Barley ◽  
Equilibrium Density ◽  
Zero Tillage ◽  
Clay Loam ◽  
Cone Resistance

SUMMARYSoil responses to deep (30–35 cm) and normal (15–20 cm) mouldboard ploughing, chisel ploughing and zero-tillage have been compared for 7 years in a field experiment growing continuous spring barley near Edinburgh. The soil was of variable texture, from moderately well-drained sandy loam overlying loam to imperfectly to poorly drained sandy clay loam overlying clay loam, classified as stagnogleyic brown earth to cambio stagnogley soil. Soils of this type derived from Carboniferous till are widely used for cereal production in south-east Scotland. Measurements of soil physical properties were made at crop emergence, midseason and at harvest to characterize seasonal and long-term responses to tillage and traffic. After the first 3 years bulk density responses varied little within or between seasons, showing a compacted horizon from 0–15 cm under zero-tillage and a looser horizon from 21–33 cm under deep ploughing compared with normal ploughing. Immediately below the depth of normal ploughing there was no difference in bulk density between this treatment and zero-tillage while in some years the chisel-ploughing treatment was denser. Moisture content responses on a weight basis, together with air-filled porosity responses, showed large differences between treatments particularly at the time of crop emergency, indicating substantial alterations in the soil profile hydrology. Expressed on a volume basis the increased moisture content near the surface under zero-tillage became more pronounced and the other effects disappeared. Cone resistance responses were proportionately larger than those for bulk density and showed one major difference in that below the depth of ploughing cone resistance was greater for zero-tillage than normal ploughing in the sixth and seventh seasons, but not previously. For bulk density, but probably not for cone resistance, there were no increases after the third season of zero-tillage, the soil reaching an equilibrium density for the current management practices and machinery usage.

scholarly journals Assessment of Seasonal Variation in Physicochemical Characteristics of the Soil at Gautala Reserve Forest (M.S), India

2020 ◽  
pp. 290-304
Author(s):  
Amrin Naimoddin Mirza ◽  
Satish S Patil
Keyword(s):  
Electrical Conductivity ◽  
Organic Carbon ◽  
Moisture Content ◽  
Physicochemical Parameters ◽  
Sandy Loam ◽  
Soil Parameters ◽  
Available Phosphorus ◽  
Available Nitrogen ◽  
Available N ◽  
Reserve Forest

The aim of study was to investigate the seasonal changes of physicochemical parameters in the soil of selected 15 spots of the Gautala reserve forest. The soil is consist of the most significant natural factors, which is created by weathering of the rocks existing in the environment. The present survey was made to study consists the physicochemical parameters in the soil of the Gautala Reserve Forest during the year 2017-18 at three seasonal intervals i.e. rainy, winter and summer seasons. The soil parameters examined were soil pH, soil texture, moisture content, bulk density, electrical conductivity (EC),organic carbon (OC), available Nitrogen (N), available Phosphorus (P), and available Potassium (K). The Gautala forest soil physical property was analyzed as sandy loam and silty loam. The pH and Organic carbon levels were low during summer and high in monsoon. The total amount of available N, P, K, electrical conductivity, water holding capacity and moisture content were maximum in monsoon and minimum in summer season. The physicochemical properties are dependent variables that play an important role in order to understand plant diversity.

scholarly journals A Study of Some Physical Properties of Two Different Soil Textures Planted with Conocarpus Trees (Conocarpuslancifolius. Engl)

2018 ◽  
Vol 7 (2) ◽  
pp. 133-145
Author(s):  
Nuhad S. S. AL- Wali ◽  
Kawthar A. AL- Mosawi
Keyword(s):  
Moisture Content ◽  
Bulk Density ◽  
Sandy Loam ◽  
Soil Depth ◽  
Penetration Resistance ◽  
Soil Samples ◽  
Silty Clay ◽  
Soil Penetration Resistance ◽  
Unplanted Soil ◽  
Mean Weight Diameter

This research has been conducted to study the effect of Conocarpus trees and their roots on some of soilphysical properties. The soil physical properties are moisture content , bulk density , total porosity , mean weight diameter (dry sieveing) and soil penetration resistance . Some soil samples are collected from two locations :the first location is Agric. College research, Garmat Ali, stations , Basra university , and the second location isZuwber province farm . The soil texture of the first location is silty clay which is classified as fine clay mixed Calcarioushy perthermictypictorrifluvent, while the soil texture of  the second location is sandy loam. This soil is classified with in species Entisol and under species psamments and high group , underhigh group and family (Typictorripsamments, Calcarious Mixed Hyperthermic).  The soil samples are collected from two soil depths( 0 – 30 and 30 – 60) from both locations are planted with Conocarpus trees, their ages ranged between 4 to 5 years . The trees height is 2.5 – 3.0 m . Another soil samples are also collected from unplanted soil  with Conocarpus trees. The results reveated that the silty clay soil is significantly surpassed the sandy loam soil in moisture content and mean weight diameter by a percentage of 68.76% and 32.91% respectively . Whereas, the bulk density and soil penetration resistance decreased , while the total porosity of the silty clay soil as compared with sandy loam soil .For unplanted soil, moisture content, the bulk density and the soil penetration resistance are increased as compared with planted soil . The soil depth (30 – 60)cm is surpassed soil depth of ( 0- 30)cm in giving higher values of moisture content andbulk density whereas it does not significantly affect the mean weight diameter and  soil penetration resistance .

scholarly journals SIFAT FISIK GAMBUT PEDALAMAN PADA LABORATORIUM ALAM HUTAN GAMBUT SEBANGAU, KALIMANTAN TENGAHThe Physical Properties Of Inland Peat In Natural Laboratory Of Peat Swamp Forest (LAHG) Sebangau, Central Kalimantan

2021 ◽  
Vol 15 (2) ◽  
pp. 216
Author(s):  
Yonodius Paskalis Bay ◽  
Nina Yulianti ◽  
Suparno Suparno ◽  
Fengky Florante Adji ◽  
Zafrullah Damanik ◽  
...  
Keyword(s):  
Hydraulic Conductivity ◽  
Moisture Content ◽  
Land Cover ◽  
Physical Properties ◽  
Bulk Density ◽  
Black Soil ◽  
Fiber Content ◽  
Soil Color ◽  
Central Kalimantan ◽  
Peat Area

Indonesia has the largest peat area in the tropical zone, which estimated about 21 million ha, with a percentage of 70% of the peat area in Southeast Asia and 50% of the world's tropical peatlands. This study aims to evaluate the physical properties of soil in each layer of soil and land cover in inland peat swamp forests in LAHG in Central Kalimantan. The research used the profile method (minipit) measuring 120 cm x 120 cm. Each location is given 3 plots on 2 (two) land cover  namely forest and burnt area. The research location is in LAHG. This research was conducted in July-December 2020. Samples were analyzed at the Banjarbaru Research and Development Laboratory. The parameters observed were bulk density, moisture content, fiber content, soil color, infiltration, and hydraulic conductivity. The research data were analyzed statistically by means of regression and correlation analysis. The results showed that the study of the physical properties of inland peat soil in the forest had bulk density ranging from 0.10 to 0.15 g / cm-3, moisture content 541.18-910.00%, fiber content 8-40%, infiltration -0 , 58-29.27 ml / hour, hydraulic conductivity 2.4-66.6 cm / hour with reddish black soil color. Whereas on burnt land, bulk density ranged from 0.10 to 0.15 g / cm-3, moisture content was 500.00-916.67%, fiber content was 12-52%, infiltration was -3.19-60.99 ml. / hr, hydraulic conductivity 2.4-30.6 cm / hr with dark black soil color. The study relationship pattern shows positive and negative.

scholarly journals Estimation on migration characteristics of leachate using analysis of hydraulic conductivity at bioreactor landfill

2019 ◽  
Vol 38 (1) ◽  
pp. 59-68
Author(s):  
Hyeong-Jin Choi ◽  
Yong Choi ◽  
Seung-Whee Rhee
Keyword(s):  
Hydraulic Conductivity ◽  
Moisture Content ◽  
Bulk Density ◽  
Recirculation Zone ◽  
Migration Time ◽  
Bioreactor Landfill ◽  
Leachate Recirculation ◽  
Factors Affecting ◽  
Recirculation Zones ◽  
The Relationship

In bioreactor landfill, moisture content is one of the most important factors affecting the migration of leachate. The migration characteristics of leachate in the Sudokwon landfill site was estimated by examining relationships among self-loading weight of waste (waste weight load), bulk density, hydraulic conductivity and moisture content of the landfilled waste. Experimental zones in the Sudokwon landfill were divided into leachate recirculation zones (3-C and 4-C zone) and reference zone (3-D zone). The volume of the leachate recirculation was 207 m3 d-1 for 12 months in the 3-C zone and 190 m3 d-1 for 3 months in the 4-C zone. A logarithmic graph can describe the relationship between waste weight load and bulk density by moisture content. However, both the relationship between bulk density and hydraulic conductivity and the relationship between hydraulic conductivity and waste weight load can be expressed by an exponential graph. Through these relationships, generalised equations for hydraulic conductivity were established using moisture content and waste weight load. The hydraulic conductivity calculated from the generalised equation in the leachate recirculation zone was estimated to be 6.27 × 10-4 cm s-1 in the 3-C zone and 4.43 × 10-4 cm s-1 in the 4-C zone. The migration time of leachate in the leachate recirculation zone was estimated to be 64.2 days in the 3-C zone and 94.5 days in the 4-C zone, respectively.

scholarly journals Variability of soil physical and hydraulic properties along a toposequence in the coastal lowlands of Rio de Janeiro

2021 ◽  
Vol 16 (1) ◽  
pp. 1
Author(s):  
João Henrique Gaia-Gomes ◽  
Carlos Roberto Pinheiro Junior ◽  
Marcos Gervasio Pereira ◽  
Wilk Sampaio de Almeida ◽  
Geuzimar Terração Silva
Keyword(s):  
Hydraulic Conductivity ◽  
Moisture Content ◽  
Bulk Density ◽  
Rio De Janeiro ◽  
Hydraulic Properties ◽  
Principal Component ◽  
Clay Content ◽  
Root Penetration ◽  
Forest Fragment ◽  
Coastal Lowlands

Soil physical and hydraulic properties are interdependent, and soil-use planning and management are complicated by the high variability of these attributes. The current study assessed the variability of physical and hydraulic properties of soils along a toposequence located in a forest fragment under spontaneous regeneration in the coastal lowlands of Rio de Janeiro. Four soil profiles were selected, and samples were collected from surface and subsurface horizons for determination of moisture content, bulk density, macroporosity, microporosity, hydraulic conductivity, texture, and soil resistance to penetration (measured using benchtop and field penetrometers). Exploratory and principal component analyses were performed, and descriptive parameters and Pearson’s correlation coefficients were calculated. In A horizons of profiles 3 (Planossolo) and 4 (Gleissolo), clay contents ranged from 59.0 to 577.0 g kg-1, moisture contents from 1.5 to 16.4%, and microporosity from 10.4 to 46.2%, respectively. Field- and laboratory-measured penetration resistances showed a stronger association with profile 1 (Argissolo); however, values were not sufficiently high to limit root development. The variability in soil physical and hydraulic properties in short slopes is high, mainly in terms of hydraulic conductivity, moisture, microporosity, and clay content. The greater variability of soil physical and hydraulic properties in lowland is attributed to clay and silt fractions, microporosity, and moisture content. The increment in clay content with depth increases bulk density and resistance to root penetration.

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